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Wetting Behavior of Iron–Carbon Melt in Silicates at Mid-Mantle Pressures With Implications for Earth’s Deep Carbon Cycle

机译：在地幔压力下硅酸盐在硅酸盐中润湿行为，具有对地球的深度碳循环的影响

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Junjie Dong; Jie Li; Feng Zhu;
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1. Partitioning of carbon between Fe-rich alloy melt and silicate melt in a magma ocean-Implications for the abundance and origin of volatiles in Earth, Mars, and the Moon [J] . Han Chi, Rajdeep Dasgupta, Megan S. Duncan, Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society . 2014,第Null期

机译：岩浆海洋中富铁合金熔体和硅酸盐熔体之间碳的分配-对地球，火星和月球中挥发物的含量和来源的影响
2. Iron spin state in silicate glass at high pressure: Implications for melts in the Earth's lower mantle [J] . C. Prescher, C. Weigel, C. McCammon, Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2014,第Null期

机译：硅酸盐玻璃在高压下的铁自旋态：对地球下地幔融化的影响
3. Use of Platinum Capsules in the Study of the Carbon and Hydrogen Solubility in Silicate Melts in Equilibrium with Liquid Iron Alloys at High Pressures and Temperatures [J] . A. A. Kadik, N. A. Kurovskaya, Yu. A. Ignatev Geochemistry International . 2013,第12期

机译：铂胶囊在高压和高温下与液态铁合金平衡研究硅酸盐熔体中碳氢溶解度的研究
4. Structural properties of sodium-rich carbonate-silicate melts: An in-situ high-pressure EXAFS study on Y and Sr [C] . J Pohlenz, S Pascarelli, O Mathon, International Conference on X-ray Absorption Fine Structure . 2015

机译：富含钠碳酸钠 - 硅酸盐的结构性质：原位高压EXAFS对Y和SR进行研究
5. An examination of the reactivity of CO2 with Mg-silicates at pressures and temperatures of the earth's mantle and implications for deep carbon storage. [D] . Devers, Emily S. 2016

机译：在地幔的压力和温度下检查CO2与Mg-硅酸盐的反应性及其对深层碳储存的影响。
6. Metastable silica high pressure polymorphs as structural proxies of deep Earth silicate melts [O] . E. Bykova, M. Bykov, A. Černok, -1

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7. Phase Diagrams of Carbonate Materials at High Pressures, with Implications for Melting and Carbon Cycling in the Deep Earth [O] . Konstantin Litasov, Anton Shatskiy, Ivan Podborodnikov, 2020

机译：高压碳酸盐材料的相图，对深土熔化和碳循环的影响

Wetting Behavior of Iron–Carbon Melt in Silicates at Mid-Mantle Pressures With Implications for Earth’s Deep Carbon Cycle

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